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The occurrence o/strong earthquakes (~6,3) and the evolution of the stress field along the southwestern part ofthe Hellenic arc since 1959 are examined by the cal­ culation of Coulomb stress changes. The study area is characterized by low angle thrust faults and high seismicity as being part ofthe subduction interface. Coulomb stress changes were calculated assuming that earthquakes can be modeled as static dislocations in an elastic hal/-space, considering the co-seismic slip during strong events and the slow tectonic stress build-up along major fault segments due to the movements 0/ the tectonic plates. The ruptures are modeled taking into account the strike, dip, and rake appropriate to each event examined. It is evaluated whether the stress changes brought a given earthquake closer to, or farther away from, failure. 1t was found that the majority o/the events (strong and smaller) are located in stress enhanced areas,

STRESS INTERACTION BETWEEN THRUST FAULTS ALONG THE SW HELLENIC ARC (GREECE)